David R. Tappin
About
In The Last Decade
David R. Tappin
74 papers receiving 3.2k citations
Hit Papers
Peers
Comparison fields: 5 of 73
- Geophysics 2.4k
- Earth-Surface Processes 1.3k
- Atmospheric Science 1.2k
- Management, Monitoring, Policy and Law 632
- Environmental Chemistry 513
Countries citing papers authored by David R. Tappin
This map shows the geographic impact of David R. Tappin's research. It shows the number of citations coming from papers published by authors working in each country. You can also color the map by specialization and compare the number of citations received by David R. Tappin with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites David R. Tappin more than expected).
Fields of papers citing papers by David R. Tappin
This network shows the impact of papers produced by David R. Tappin. Nodes represent research fields, and links connect fields that are likely to share authors. Colored nodes show fields that tend to cite the papers produced by David R. Tappin. The network helps show where David R. Tappin may publish in the future.
Co-authorship network of co-authors of David R. Tappin
This figure shows the co-authorship network connecting the top 25 collaborators of David R. Tappin. A scholar is included among the top collaborators of David R. Tappin based on the total number of citations received by their joint publications. Widths of edges represent the number of papers authors have co-authored together. Node borders signify the number of papers an author published with David R. Tappin. David R. Tappin is excluded from the visualization to improve readability, since they are connected to all nodes in the network.
All Works
| # | Work | Indexed citations |
|---|---|---|
| 1 | 35 | |
| 2 | 25 | |
| 3 | Modelling of the tsunami from the December 22, 2018 lateral collapse of Anak Krakatau volcano in the Sunda Straits, Indonesia breakdown → | 198 |
| 4 | The devastating eruption tsunami of Anak Krakatau - 22nd December 2018 | 1 |
| 5 | Modeling of the slide and tsunami generation from the 12/22/18 lateral collapse of Anak Krakatau volcano (Sunda Straits, Indonesia): comparison with recent field surveys of slide deposits and tsunami impact | 2 |
| 6 | 14 | |
| 7 | Modeling of the Tohoku-oki 2011 tsunami coastal hazard: effects of a mixed co-seismic and seabed failure source | 1 |
| 8 | 43 | |
| 9 | The 1908 Messina tsunami. Some comments on the source: earthquake, submarine landslide or a combination of both? | 6 |
| 10 | 8 | |
| 11 | Contrasting styles of deformation along the Sumatra subduction zone | 1 |
| 12 | Imaging the Rupture Areas of the Giant Northern Sumatra Earthquakes: A Multidisciplinary Geophysical Experiment | 4 |
| 13 | Forearc morphology and thrust vergence, Sunda subduction zone | 4 |
| 14 | Thrust Sheet Emplacement at the Northern Sumatra Margin New Insights from the SeaCause Multichannel Reflection Seismic Experiment | 1 |
| 15 | Recent seafloor deformation at the 26 December 2004 Indian Ocean earthquake rupture zone: results from the HMS Scott 2005 survey (abstract of paper presented at the EGU General Assembly 2005, Vienna, 24-29 April 2005) | 2 |
| 16 | Evidence for Seafloor Deformation During Great Subduction Zone Earthquakes of the Sumatran Subduction zone: Results From the First Seafloor Survey Onboard the HMS Scott, 2005 | 3 |
| 17 | An Overview of SEATOS: Sumatra Earthquake and Tsunami Offshore Survey | 1 |
| 18 | 10 | |
| 19 | 10 | |
| 20 | Megatsunami Deposits on the Island of Hawaii: Implications for the Origin of Similar Deposits in Hawaii and Confirmation of the `Giant Wave Hypothesis' | 2 |
Rankless uses publication and citation data sourced from OpenAlex, an open and comprehensive bibliographic database. While OpenAlex provides broad and valuable coverage of the global research landscape, it—like all bibliographic datasets—has inherent limitations. These include incomplete records, variations in author disambiguation, differences in journal indexing, and delays in data updates. As a result, some metrics and network relationships displayed in Rankless may not fully capture the entirety of a scholar's output or impact.